A shadow instrument
Why does a tree’s shadow move and change length?
Move the Sun and watch the shadow of a marked point 5 metres above level ground.
Height above the horizon
Clockwise from north: N 0° · E 90° · S 180° · W 270°
- Shadow length
- 5.00 m
- Shadow bearing
- 315°
Follow the light to the ground
The shadow points away from the Sun. Lower sunlight meets the ground farther from the reference, making a longer shadow. Moving the Sun around the horizon changes the shadow’s direction. At a fixed elevation, that rotation does not change its length.
Geometry, assumptions, and sources
In the right triangle, tan(elevation) = height ÷ shadow length. Rearranging gives shadow length = height ÷ tan(elevation).
The reference is upright on level ground and sunlight is parallel. The tree model provides context; its canopy shadow is not calculated. This experiment omits canopy gaps, soft edges, slopes, weather, and atmospheric refraction. The independent controls do not reproduce a daily or seasonal solar path. The rim pointer shows horizontal Sun direction, not the Sun’s physical height or distance.
- NOAA: azimuth and elevation definitions
- NASA: shadow geometry, page 4 (local geometry from a lunar-lighting document)
- NOAA: observing shadows